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  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2011
    In:  Geophysical Research Letters Vol. 38, No. 14 ( 2011-07), p. n/a-n/a
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 38, No. 14 ( 2011-07), p. n/a-n/a
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2011
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    IWA Publishing ; 1993
    In:  Water Science and Technology Vol. 27, No. 2 ( 1993-01-01), p. 25-36
    In: Water Science and Technology, IWA Publishing, Vol. 27, No. 2 ( 1993-01-01), p. 25-36
    Abstract: A mathematical model was developed to describe the dynamic behaviour of the anaerobic mesophilic digestion. Special emphasis was given to the acetate degradation kinetics, as the step that determines the stability of anaerobic digestion. From the safety factor (maximum/average degradation rate) of acetate degradation in the range of 5.3 to 23 days hydraulic detention time, a maximum observed growth rate of 0.37 d−1 and decay rate of 0.10 d−1 were estimated. Temperature and pH dependence of acetate conversion was also determined and included in the model. The model was verified with load variation experiments on laboratory and full scale digesters. Mesophilic digestion with anaerobic thermophilic pretreatment is more sensitive to load variation than single mesophilic digestion. However two stage treatment leads to better sludge characteristics (thickening, viscosity, COD, TSS) of the treated sludge.
    Type of Medium: Online Resource
    ISSN: 0273-1223 , 1996-9732
    Language: English
    Publisher: IWA Publishing
    Publication Date: 1993
    detail.hit.zdb_id: 764273-8
    detail.hit.zdb_id: 2024780-1
    SSG: 14
    Location Call Number Limitation Availability
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  • 3
    Online Resource
    Online Resource
    Society of Rheology ; 2020
    In:  Journal of Rheology Vol. 64, No. 1 ( 2020-01), p. 141-160
    In: Journal of Rheology, Society of Rheology, Vol. 64, No. 1 ( 2020-01), p. 141-160
    Type of Medium: Online Resource
    ISSN: 0148-6055 , 1520-8516
    Language: English
    Publisher: Society of Rheology
    Publication Date: 2020
    detail.hit.zdb_id: 1461060-7
    Location Call Number Limitation Availability
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  • 4
    Online Resource
    Online Resource
    Copernicus GmbH ; 2010
    In:  Natural Hazards and Earth System Sciences Vol. 10, No. 7 ( 2010-07-01), p. 1379-1391
    In: Natural Hazards and Earth System Sciences, Copernicus GmbH, Vol. 10, No. 7 ( 2010-07-01), p. 1379-1391
    Abstract: Abstract. A climatology of cyclones with a focus on their relation to wind storm tracks in the Mediterranean region (MR) is presented. Trends in the frequency of cyclones and wind storms, as well as variations associated with the North Atlantic Oscillation (NAO), the East Atlantic/West Russian (EAWR) and the Scandinavian variability pattern (SCAND) are discussed. The study is based on the ERA40 reanalysis dataset. Wind storm tracks are identified by tracking clusters of adjacent grid boxes characterised by extremely high local wind speeds. The wind track is assigned to a cyclone track independently identified with an objective scheme. Areas with high wind activity – quantified by extreme wind tracks – are typically located south of the Golf of Genoa, south of Cyprus, southeast of Sicily and west of the Iberian Peninsula. About 69% of the wind storms are caused by cyclones located in the Mediterranean region, while the remaining 31% can be attributed to North Atlantic or Northern European cyclones. The North Atlantic Oscillation, the East Atlantic/West Russian pattern and the Scandinavian pattern all influence the amount and spatial distribution of wind inducing cyclones and wind events in the MR. The strongest signals exist for the NAO and the EAWR pattern, which are both associated with an increase in the number of organised strong wind events in the eastern MR during their positive phase. On the other hand, the storm numbers decrease over the western MR for the positive phase of the NAO and over the central MR during the positive phase of the EAWR pattern. The positive phase of the Scandinavian pattern is associated with a decrease in the number of winter wind storms over most of the MR. A third of the trends in the number of wind storms and wind producing cyclones during the winter season of the ERA40 period may be attributed to the variability of the North Atlantic Oscillation.
    Type of Medium: Online Resource
    ISSN: 1684-9981
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2010
    detail.hit.zdb_id: 2069216-X
    detail.hit.zdb_id: 2064587-9
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